Use of an internal standard with differential X-ray diffraction analysis for iron oxides.

Ray B. Bryant, N. Curi, C. B. Roth, D. P. Franzmeier

Research output: Contribution to journalArticle

7 Citations (Scopus)

Abstract

In the differential X-ray diffraction (DXRD) method the diffraction pattern for iron minerals in a soil or clay sample is obtained by subtracting the pattern for a sample free of iron oxides, after appropriate adjustment of intensity, from that of an untreated sample. We modified this method by using alumina as an internal standard to calculate the scale factor for the adjustment of intensity. The internal standard also serves as a reference for making corrections in peak position.-from Authors

Original languageEnglish (US)
Pages (from-to)168-173
Number of pages6
JournalSoil Science Society of America Journal
Volume47
Issue number1
DOIs
StatePublished - Jan 1 1983

Fingerprint

iron oxides
X-ray diffraction
iron oxide
aluminum oxide
diffraction
sampling
iron
clay
mineral soils
mineral
soil
methodology
analysis
method

All Science Journal Classification (ASJC) codes

  • Soil Science

Cite this

Bryant, Ray B. ; Curi, N. ; Roth, C. B. ; Franzmeier, D. P. / Use of an internal standard with differential X-ray diffraction analysis for iron oxides. In: Soil Science Society of America Journal. 1983 ; Vol. 47, No. 1. pp. 168-173.
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Use of an internal standard with differential X-ray diffraction analysis for iron oxides. / Bryant, Ray B.; Curi, N.; Roth, C. B.; Franzmeier, D. P.

In: Soil Science Society of America Journal, Vol. 47, No. 1, 01.01.1983, p. 168-173.

Research output: Contribution to journalArticle

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